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were analyzed according to the Coastal Change Analysis Program (C-CAP) protocol
to determine land cover and a subsequent change detection. The data were field
validated and mosaicked to produce a land cover inventory for Northern Maine.
If you wish to create an attribute table to identify the different land cover
classifications, an easy reference table is available under the PROCESS
DESCRIPTION section.</gco:CharacterString>
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            <gco:CharacterString>To improve the understanding of coastal uplands and wetlands, and
their linkages with the distribution, abundance, and health of living marine
resources.

SPATIAL DATA ORGANIZATION INFORMATION 
Direct Spatial Reference: Raster

SPATIAL REFERENCE INFORMATION - PLANAR 
Grid Coordinate System Name: Universal Transverse Mercator
UTM Zone Number: 19
Scale Factor at Central Meridian: 1
Longitude of Central Meridian: -69
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False Northing: 0.00000
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Abscissa Resolution: 30
Ordinate Resolution: 30
Planar Distance Units: Meters

SPATIAL REFERENCE INFORMATION - GEODETIC MODEL 
Horizontal Datum Name: North American Datum 1983
Ellipsoid Name: GRS80
Semi-major Axis: 6378206.4
Denominator of Flattening Ratio: 294.98

NATIVE: ERDAS IMAGINE Version 8.2 on a SUN Sparc-10 using SUN Operating System
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      ACCESS CONSTRAINTS: None, except for a possible fee at the cost of
      reproduction.
      
      DISTRIBUTION LIABILITY: Users must assume responsibility to determine the
      usability of these data. 
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      Data set is not for use in litigation. While efforts have been made to ensure
      that these data are accurate and reliable within the state of the art, NOAA,
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      inaccuracies in the data, or as a result of the data to be used on a particular
      system. NOAA makes no warranty, expressed or implied, nor does the fact of
      distribution constitute such a warranty. Additional Use Constraints: This data
      set was the second C-CAP Analysis completed and still considered a prototype.
      No accuracy assessment was performed on this data set and no accuracy
      assessment statistics are available.
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                                    <gco:CharacterString>Olsen, L.M., G. Major, K. Shein, J. Scialdone, R. Vogel, S. Leicester, H. Weir, S. Ritz, T. Stevens, M. Meaux, C.Solomon, R. Bilodeau, M. Holland, T. Northcutt, R. A. Restrepo, 2007 .   NASA/Global Change Master Directory (GCMD) Earth Science Keywords. Version  6.0.0.0.0</gco:CharacterString>
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      ATTRIBUTE ACCURACY REPORT: A team of field investigators participated in data
      verification exercises on UNKNOWN. Data validation teams consisted of personnel
      from the Data validation teams consisted of personnel from the Gulf of Maine
      Program, the U.S. Fish and Wildlife Service, Environment Canada, Moosehorn
      Wildlife Refuge, Georgia Pacific, the Oak Ridge National Laboratory, and the
      NOAA Coastal Services Center. Each team was equipped with a portable color
      laptop computer linked to a Global Positioning System (GPS). The field station
      runs software that supports the classified data as a raster background with the
      road network as a vector overlay with a simultaneous display of live GPS
      coordinates. Accuracy assessment points were generated with ERDAS Imagine
      software using a stratified random sample in 3x3 pixel homogeneous windows. To
      make the acquisition of the field reference data more practical, a twenty pixel
      buffer area around roads (i.e. 10 pixels on each side of the road) was created.
      668 random points were generated within this area for the accuracy assessment.
      Collection of ground reference information for areas that have experienced a
      change in land cover type is a troublesome task. Pre-Processing Steps: The
      scene was georectified to UTM Zone 19 coordinates. Ancillary data sets:
      Subsequent field work and the use of collateral data such as USGS maps, county
      marsh inventories, and National Wetland Inventory data led to further
      refinements in the image classification. Shoreline features can be extracted
      from Landsat images by detecting the land/water interface. However, care must
      be used to avoid misinterpreting tidal differences as changes in shorelines,
      since the satellite images from which these land cover images are derived and
      acquired at different tidal stages, depending on when the satellite is
      overhead. The land cover classifications represent the instantaneous state of
      the shoreline at the moment of image acquisition. C-CAP data are mapped at
      1:100,000 scale with 22 standard classes constituting major landscape
      components. They are not jurisdictional (can't be used for permitting) and will
      not identify individual species. However, they are useful for identifying
      regional landscape patterns, major functional niches, environmental impact
      assessment, urban planning, and zoning applications. If you need change
      analysis data at this scale, C-CAP may be your only option. C-CAP is designed
      around a 1 to 5 year revisit cycle. Land Cover is the complete human and
      natural landscape recorded as surface components - forest, water, wetlands,
      concrete, asphalt, etc. Land cover can be documented by analyzing spectral
      signatures of satellite and aerial imagery. Land Use is the documentation of
      human uses of the landscape - residential, commercial, agricultural, etc. Land
      use can be inferred but, not explicitly derived from satellite and aerial
      imagery. There is no spectral basis for land use determination in satellite
      imagery. C-CAP data can be used to identify concrete and asphalt as land cover,
      but we can only infer that these materials denote a residential or commercial
      use. Post-Processing Steps: The data were put through a datum conversion from
      UTM NAD27 to UTM NAD83 zone 19. Known Problems: None Accuracy Results: None
      performed, therefore unknown, refer to Use Constraints for more information. 
      
      LOGICAL CONSISTENCY REPORT: Tests for logical consistency indicate that all row
      and column positions in the selected latitude/longitude window contain data.
      Conversion and integration with vector files indicates that all positions are
      consistent with earth coordinates covering the same area. Attribute files
      appear to be logically consistent. Examining the change matrix for logical
      fallacies, we find, for example, that a very small number of pixels changed
      from developed land to any other category. 
      
      COMPLETENESS REPORT: The classification scheme comprehensively includes all
      anticipated land covers, and all pixels have been classified. The NOAA Coastal
      Change Analysis Program (C-CAP): Guidance for Regional Implementation, NOAA
      National Marine Fisheries Service Report 123, discusses the interagency effort
      to develop the land cover classification scheme and defines all categories. 
      
      HORIZONTAL POSITIONAL ACCURACY REPORT: Precision corrected images were
      purchased from the EROS Data Center in UTM NAD27 meters to an RMSE +/- 0.5
      pixels. 
      
      VERTICAL POSITIONAL ACCURACY REPORT: There was no terrain correction in the
      georeferencing procedure. 
      
      PROCESS DESCRIPTION: The processing steps for each C-CAP Northern Maine Land
      Cover 1992 Analysis product are intricately associated. Each database is the
      result of many processing steps with numerous iterations for each step. The
      output of one processing step or database is often the input data for another
      processing step. A brief description of the processing steps used in the land
      cover classification of the this project follows. Further description of the
      processing steps can be found in the NOAA Coastal Change Analysis Program
      (C-CAP): Guidance for Regional Implementation, NOAA National Marine Fisheries
      Service Report 123 (Dobson et al, 1995). Baseline Classification Process: The
      Northern Maine land cover/change classification product was processed using an
      iterative classification approach. Landsat Thematic Mapper data for
      path/row/date(s): 10/29 19920526 were analyzed and mosaicked to create a land
      cover for Northern Maine. The scene was classified, focusing first on
      separating major categories (e.g. water, forest, marsh, herbaceous upland, and
      developed) using standard supervised classification techniques. Numerous
      individual areas were chosen as training sites for the land cover
      classification. The mean and covariance statistics for these areas are passed
      to an isodata classification algorithm which assigns an unknown pixel to the
      class in which it has the highest probability of being a member. Then iterative
      unsupervised classifications were performed on each major category individually
      by masking out all other major categories. With this type of unsupervised
      classification, the computer is allowed to query the multispectral properties
      of the masked scene using user specified criteria and to identify X mutually
      exclusive clusters in N-dimensional feature space. By masking out all data but
      a single major category, the spectral variance is greatly reduced thus
      decreasing classification errors. After several classification iterations of
      the masked data, final classification labels were assigned to the spectral
      clusters. Changes among major categories were permitted to occur even at this
      stage of processing. Subsequent field work and the use of collateral data such
      as USGS maps, TIGER road data, and National Wetland Inventory data led to
      further refinements in the image classification. In small areas where landcover
      class confusion could not be separated spectrally, human pattern recognition
      was used to recode the data. A spatial filter was applied to the final
      classification data file. Change Classification Process: Landsat Thematic
      Mapper data for path/row(s) 10/29 19920526 were analyzed to arrive at a land
      cover for Northern Maine. The change date land cover classification was in part
      derived from the baseline classification. Only the pixels in the May 26, 1992
      image that changed spectrally from the change date image were classified for
      the May 23, 1985 data file. All other pixels were simply replaced with the
      baseline image classification. It is possible to simply identify the amount of
      change between two images by image differencing the same band in two images
      which have previously been rectified to a common basemap. Image differencing
      involves subtracting the imagery of one date from that of another. The
      subtraction results in positive and negative values in areas of radiance change
      and zero values in areas of no-change in a new 'change image'. The images are
      subtracted resulting in an signed 16-bit analysis with pixel values ranging
      from -255 to 255. The results were transformed into positive unsigned 16-bit
      values by adding a constant, c. The operation is expressed mathematically as:
      Dijk = BVijk(1) - BVijk(2) + c where Dijk = change pixel value BVijk(1) =
      brightness value at time 1 BVijk(2) = brightness value at time 2 c = a constant
      (e.g., 255). i = line number j = column number k = a single band (e.g. TM band
      4). The 'change image' produced using image differencing usually yields a BV
      distribution approximately gaussian in nature, where pixels of no BV change are
      distributed around the mean and pixels of change are found in the tails of the
      distribution. A threshold value was carefully chosen to identify spectral
      'change' and 'no-change' pixels in the 'change image.' A 'change/no-change'
      mask was derived by performing image differencing on band 4, and Normalized
      Difference Vegetation Index (NDVI) of the two date dataset and recoded into a
      binary mask file. The 'change/no-change' mask was then overlaid onto the
      earlier date of imagery and only those pixels which were detected as having
      spectrally changed were viewed as candidate pixels for categorical change.
      Change Detection Database The change date and baseline land cover
      classifications were compared on a pixel by pixel basis using a change
      detection matrix. This traditional post-classification comparison yields 'from
      land cover class - to land cover class' change information. Many pixels with
      sufficient change to be included in the mask of candidate pixels in the
      spectral change process did not qualify as categorical land cover change. This
      method may reduce change detection errors (omission and commission) and
      provides detailed 'from-to' change class information. The technique reduces
      effort by allowing analysts to focus on the small amount of area that has
      changed between dates. PROCESS DATE: 19940930
      
      PROCESS DESCRIPTION: This data was projected to Universal Transverse Mercator
      zone 19 with a horizontal datum of NAD83. PROCESS DATE: Unknown
      
      SOURCE INFORMATION - CITATION: Earth Observation Satellite Company. Landsat
      Thematic Mapper Source_Geospatial_Data_Presentation_Form: remote-sensing image.
      1992-05-26. OTHER CITATION DETAILS: Landsat Thematic Mapper scenes processed:
      Path = 10 Row = 29 Date 05-26-1992 
      TYPE OF SOURCE MEDIA: 8 mm magnetic tape. 
      SOURCE CURRENTNESS REFERENCE: ground condition. 
      SOURCE CITATION ABBREVIATION: north_85. 
      SOURCE CONTRIBUTION: Source used in land cover classification.
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